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Using MODIS derived fPAR with ground based flux tower measurements to derive the light use efficiency for two Canadian peatlands

Connolly, John (författare)
University College Dublin
Roulet, Nigel T. (författare)
McGill University
Seaquist, Jonathan (författare)
Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science
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Holden, N. M. (författare)
University College Dublin
Lafleur, Peter M. (författare)
Trent University
Humphreys, Elyn R (författare)
Carleton University
Heumann, B. W. (författare)
University of North Carolina
Ward, S. M. (författare)
University College Dublin
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 (creator_code:org_t)
2009-02-19
2009
Engelska 234 s.
Ingår i: Biogeosciences. - : Copernicus GmbH. - 1726-4189. ; 32:6, s. 225-225
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • We used satellite remote sensing data; fractionof photosynthetically active radiation absorbed by vegetation(fPAR) from the Moderate Resolution Imaging Spectrora-diometer (MODIS) in combination with tower eddy covari-ance and meteorological measurements to characterise theLight Use Efficiency parameter (ε)variability and the maxi-mumε(εmax)for two contrasting Canadian peatlands. Eight-day MODISfPAR data were acquired for the Mer Bleue(2000 to 2003) and Western Peatland (2004). Flux towereddy covariance and meteorological measurements were in-tegrated to the same eight-day time stamps as the MODISfPAR data. A light use efficiency model: GPP =ε×APAR(where GPP is Gross Primary Productivity and APAR is ab-sorbed photosynthetically active radiation) was used to cal-culateε. Theεmaxvalue for each year (2000 to 2003) at theMer Bleue bog ranged from 0.58 g C MJ−1to 0.78 g C MJ−1and was 0.91 g C MJ−1in 2004, for the Western Peatland.The average growing seasonεfor the Mer Bleue bog forthe four year period was 0.35 g C MJ−1and for the West-ern Peatland in 2004 was 0.57 g C MJ−1. The average snowfree period for the Mer Bleue bog over the four years was 0.27 g C MJ−1and for the Western Peatland in 2004 was0.39 g C MJ−1. Using the light use efficiency method wecalculated theεmaxand the annual variability inεfor twoCanadian peatlands. We determined that temperature was agrowth-limiting factor at both sites Vapour Pressure Deficit(VPD) however was not. MODISfPAR is a useful tool forthe characterization ofεat flux tower sites.

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